Abstract
Grass silica short cell phytoliths (GSSCPs), which are profusely produced within the grasses are often subfamily-specific and hence may act as one of the reliable plant proxies in deciphering eco-climatic conditions of an area. To assess how reliably grass phytolith morphs can capture the signal of rainfall variations of an area and to overcome the bias caused due to the redundancy and the multiplicity of GSSCPs, some Chloridoid grasses and soil samples from Maharashtra part of the Western Ghats along the west-east rainfall gradient are studied. The study reveals that Saddle are the dominant morphotype produced by the members of this grass subfamily irrespective of the rainfall variations. Surface soil phytolith assemblage revealed that Saddle morphs are inversely proportional to rainfall i.e., they increase with decrease in rainfall and vice versa. Based on this data, regions with MAP >2000 mm and <2000 mm could be separated in the northern Western Ghats. The results of the CCA and PCA also corroborated these observations.
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